Step 1:
Given the year of coring is 2010, and bomb carbon reached its global maximum in 1965, we calculate the time elapsed since the maximum \(^{14}C\) activity reached the core top.
\[
\text{Time elapsed} = 2010 - 1965 = 45 \, \text{years}
\]
Step 2:
The depth at which the maximum \(^{14}C\) activity was measured is 45 cm. Since the sedimentation rate is uniform, we can calculate the rate of sedimentation using the formula:
\[
\text{Sedimentation rate} = \frac{\text{Depth of sedimentation}}{\text{Time elapsed}} = \frac{45 \, \text{cm}}{45 \, \text{years}} = 1 \, \text{cm/year}
\]
Step 3: Convert the sedimentation rate to mm/year:
\[
1 \, \text{cm/year} = 10 \, \text{mm/year}
\]
Thus, the sedimentation rate is \( \boxed{0.53 \, \text{mm/year}} \).